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Bonaccorsi, E., Pasero, M. (2003) Crystal structure refinement of sahlinite Pb14(AsO4)2O9Cl4. Mineralogical Magazine, 67 (1) 15-21 doi:10.1180/0026461036710080

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Reference TypeJournal (article/letter/editorial)
TitleCrystal structure refinement of sahlinite Pb14(AsO4)2O9Cl4
JournalMineralogical Magazine
AuthorsBonaccorsi, E.Author
Pasero, M.Author
Year2003 (February)Volume67
Page(s)15-21Issue1
PublisherMineralogical Society
Download URLhttps://rruff.info/rruff_1.0/uploads/MM67_15.pdf+
DOIdoi:10.1180/0026461036710080Search in ResearchGate
Classification
Not set
LoC
Not set
Mindat Ref. ID243407Long-form Identifiermindat:1:5:243407:4
GUID69d790f7-465a-4e8b-be76-d1d14220abc3
Full ReferenceBonaccorsi, E., Pasero, M. (2003) Crystal structure refinement of sahlinite Pb14(AsO4)2O9Cl4. Mineralogical Magazine, 67 (1) 15-21 doi:10.1180/0026461036710080
Plain TextBonaccorsi, E., Pasero, M. (2003) Crystal structure refinement of sahlinite Pb14(AsO4)2O9Cl4. Mineralogical Magazine, 67 (1) 15-21 doi:10.1180/0026461036710080
Abstract/NotesThe crystal structure of sahlinite [Pb14(AsO4)2O9Cl4] from Lågban (Sweden) has been refined up to R = 0.071 using single-crystal diffraction data collected at the Elettra synchrotron facility. Sahlinite is monoclinic, space group C2/c, with a = 12.704(4), b = 22.576(5), c = 11.287(4) Å, β = 118.37(3)°. Sahlinite is isostructural with kombatite, its vanadium counterpart. Both are derivatives of the litharge form of PbO. In the structure of sahlinite there are seven independent Pb atoms, which are linked to Cl and/or O atoms, with coordination number ranging from V to VIII. The coordination polyhedra are irregularly shaped, due to the 6s2 lone-pair effect displayed by Pb2+.

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